<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-19T17:12:34Z</responseDate><request verb="GetRecord" identifier="oai:dspace.mit.edu:1721.1/58532" metadataPrefix="dim">https://dspace.mit.edu/server/oai/request</request><GetRecord><record><header><identifier>oai:dspace.mit.edu:1721.1/58532</identifier><datestamp>2022-01-20T15:04:43Z</datestamp><setSpec>com_1721.1_7582</setSpec><setSpec>com_1721.1_7581</setSpec><setSpec>col_1721.1_131023</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="advisor" lang="en_US">Reginald E. Newell.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author" lang="en_US">Richards, Merwin E</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="other" lang="en_US">Massachusetts Institute of Technology. Dept. of Meteorology.</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="department" lang="en_US">Massachusetts Institute of Technology. Department of Meteorology</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="department">Massachusetts Institute of Technology. Department of Aeronautics and Astronautics</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="department">Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2010-09-14T18:05:18Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="available">2010-09-14T18:05:18Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued" lang="en_US">1967</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">http://hdl.handle.net/1721.1/58532</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="oclc" lang="en_US">16857400</dim:field>
   <dim:field mdschema="dc" element="description" lang="en_US">Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Aeronautics and Astronautics; and, (M.S.)--Massachusetts Institute of Technology, Dept. of Meteorology, 1967.</dim:field>
   <dim:field mdschema="dc" element="description" lang="en_US">Includes bibliographical references (leaves 167-170).</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract" lang="en_US">A monthly statistical analysis was made of the effects of large scale horizontal eddy transport processes on the zonal momentum, heat and energy budgets for three layers of the 1965 stratosphere. Geostrophic wind components were computed from IQSY data at 100, 50, 30 and 10 mb for use in calculating the statistical quantities -used in the analysis. It was found that temporal and spatial variances and covariances -computed from monthly means of temperature and geostrophic wind components give meaningful results when used in the computation of momentum, heat and energy balances. Monthly meridional distributions of eddy transports and energy conversions show large latitudinal and height variations. They also indicate a physically reasonable compatibility with month to month changes in zonal mean values of temperature, zonal wind and geo-potential. It was further determined that in the winter, the eddies in the middle stratosphere convert a self contained source of zonal available potential energy into eddy available potential energy. It is speculated that further conversion of this energy eventuates in its availability as a significant source for the mean zonal motions.</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="statementofresponsibility" lang="en_US">by Merwin Eugene Richards.</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="degree" lang="en_US">M.S.</dim:field>
   <dim:field mdschema="dc" element="format" qualifier="extent" lang="en_US">x, 171 leaves</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso" lang="en_US">eng</dim:field>
   <dim:field mdschema="dc" element="publisher" lang="en_US">Massachusetts Institute of Technology</dim:field>
   <dim:field mdschema="dc" element="rights" lang="en_US">M.I.T. theses are protected by &#xd;
copyright. They may be viewed from this source for any purpose, but &#xd;
reproduction or distribution in any format is prohibited without written &#xd;
permission. See provided URL for inquiries about permission.</dim:field>
   <dim:field mdschema="dc" element="rights" qualifier="uri" lang="en_US">http://dspace.mit.edu/handle/1721.1/7582</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Aeronautics and Astronautics.</dim:field>
   <dim:field mdschema="dc" element="subject" lang="en_US">Meteorology.</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcc" lang="en_US">QC881.2.S8 R51</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh" lang="en_US">Stratosphere</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh" lang="en_US">Energy budget (Geophysics)</dim:field>
   <dim:field mdschema="dc" element="subject" qualifier="lcsh" lang="en_US">Eddy flux</dim:field>
   <dim:field mdschema="dc" element="title" lang="en_US">The energy budget of the stratosphere during 1965</dim:field>
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   	&lt;Title>The energy budget of the stratosphere during 1965&lt;/Title>
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   	&lt;PublicationDate>1967&lt;/PublicationDate>
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        	&lt;DisplayName>Richards, Merwin E&lt;/DisplayName>
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    &lt;Keyword>Aeronautics and Astronautics.&lt;/Keyword>
    &lt;Keyword>Meteorology.&lt;/Keyword>
   	&lt;Abstract>A monthly statistical analysis was made of the effects of large scale horizontal eddy transport processes on the zonal momentum, heat and energy budgets for three layers of the 1965 stratosphere. Geostrophic wind components were computed from IQSY data at 100, 50, 30 and 10 mb for use in calculating the statistical quantities -used in the analysis. It was found that temporal and spatial variances and covariances -computed from monthly means of temperature and geostrophic wind components give meaningful results when used in the computation of momentum, heat and energy balances. Monthly meridional distributions of eddy transports and energy conversions show large latitudinal and height variations. They also indicate a physically reasonable compatibility with month to month changes in zonal mean values of temperature, zonal wind and geo-potential. It was further determined that in the winter, the eddies in the middle stratosphere convert a self contained source of zonal available potential energy into eddy available potential energy. It is speculated that further conversion of this energy eventuates in its availability as a significant source for the mean zonal motions.&lt;/Abstract>
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